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The location of the state of Tennessee. Paleontology in Tennessee refers to paleontological research occurring within or conducted by people from the U.S. state of Tennessee. During the early part of the Paleozoic era, Tennessee was covered by a warm, shallow sea. This sea was home to brachiopods, bryozoans, cephalopods, corals, and trilobites.
The Coats–Hines–Litchy site (formerly Coats–Hines) is a paleontological site located in Williamson County, Tennessee, in the Southeastern United States.The site was formerly believed to be archaeological, and identified as one of only a very few locations in Eastern North America containing evidence of Paleoindian hunting of late Pleistocene proboscideans. [1]
Coon Creek (Mississippi) Named by. B. Wade. The Coon Creek Formation or Coon Creek Tongue is a geologic unit and Konservat-Lagerstätte located in western Tennessee and extreme northeast Mississippi. [1] It is a sedimentary sandy marl deposit, Late Cretaceous (Maastrichtian) in age, about 70 million years old.
Coon Creek Science Center. The Coon Creek Science Center is a science center and fossil finding site at 2985 Hardin Graveyard Road in Adamsville, McNairy County, Tennessee, US. The science center is situated on a 232 acres (94 ha) property on one of the most important fossil sites in North America. [1] The Coon Creek Formation is a geologic ...
Eva site. The Eva site (40BN12) is a prehistoric Native American site in Benton County, Tennessee, in the Southeastern United States. Located along an ancient channel of the Tennessee River, the Eva site saw extensive periods of occupation during the Middle and Late Archaic period (c. 6000-1000 BC). The site's well-defined midden layers helped ...
The Old Stone Fort is a prehistoric Native American structure located in Coffee County, Tennessee, in the Southeastern United States.Most likely built between 80 and 550 AD during the Middle Woodland period, the structure is considered the most complex hilltop enclosure found in the South and was likely used for ceremonial purposes rather than defense.
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The impact crater was formed approximately 360 million years ago as a shallow, saucer-shaped crater, 3.8 kilometres (2.4 mi) in diameter and about 150 metres (490 ft) deep. A large central hill, highly deformed rim strata, and a breccia lens 40 m (130 ft) in thickness were produced during formation. Over 2 square kilometres (490 acres) of flat ...
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